Hydrothermal fluid evolution associated with gold mineralization at the Wenyu Mine, Xiaoqinling District, China
文献类型：期刊论文
| 作者 | Jiang, N |
| 刊名 | RESOURCE GEOLOGY
 |
| 出版日期 | 2000 |
| 卷号 | 50期号:2页码:103-112 |
| 关键词 | Wenyu gold deposit Xiaoqinling mesothermal fluid inclusion fluid immiscibility H2O-CO2-NaCl liquid China |
| ISSN号 | 1344-1698 |
| 英文摘要 | The Wenyu mesothermal gold deposit is located in the Xiaoqinling district about 1000 km southwest of Beijing in central China. It occurs,in the Late Archean to Early Proterozoic metamorphosed volcanic and sedimentary rocks. Three distinct stages of veins have been identified: (I) gold-poor quartz-pyrite veins, (II) gold-rich sulfide-quartz veins, and (III) gold-poor carbonate-quartz veins. Stage II can be subdivided into IIa and IIb. Gold typically occurs as fracture-fillings associated with chalcopyrite and galena. |
| 语种 | 英语 |
| WOS记录号 | WOS:000088609200003 |
| 出版者 | SOC RESOURCE GEOLOGY |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/76083]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Jiang, N |
| 作者单位 | Chinese Acad Sci, Inst Geol & Geophys, Res Ctr Mineral Resources Explorat, Beijing 100101, Peoples R China |
| 推荐引用方式 GB/T 7714 | Jiang, N. Hydrothermal fluid evolution associated with gold mineralization at the Wenyu Mine, Xiaoqinling District, China[J]. RESOURCE GEOLOGY,2000,50(2):103-112. |
| APA | Jiang, N.(2000).Hydrothermal fluid evolution associated with gold mineralization at the Wenyu Mine, Xiaoqinling District, China.RESOURCE GEOLOGY,50(2),103-112. |
| MLA | Jiang, N."Hydrothermal fluid evolution associated with gold mineralization at the Wenyu Mine, Xiaoqinling District, China".RESOURCE GEOLOGY 50.2(2000):103-112. |
入库方式： OAI收割
来源：地质与地球物理研究所
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